Method of removing dissolved silica from waste water
20180162746 ยท 2018-06-14
Inventors
- Tina N. Nenoff (Albuquerque, NM, US)
- Koroush Sasan (Albuquerque, NM, US)
- Patrick V. Brady (Albuquerque, NM)
- James L. Krumhansl (Albuquerque, NM)
Cpc classification
B01J41/02
PERFORMING OPERATIONS; TRANSPORTING
International classification
Abstract
Dissolved silica is ubiquitous in impaired waters, a fouling agent in desalination membranes, resistant to existing antiscalants, and difficult to remove from power plant feed waters, thereby inhibiting long term reuse of industrial water. According to the present invention, an inorganic anion exchanger, hydrotalcite (HTC), can provide highly selective removal of silica from aqueous solutions. Calcined HTC effectively removes silicate anion from different waste waters and waters with high concentration of competing ions, such as SO.sub.4.sup.2 and Cl.sup.. For example, calcined Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3).4H.sub.2O has a silica adsorption capacity of 45 mg SiO.sub.2/g HTC. Further, HTC can be easily regenerated and recycled.
Claims
1. A method for removing dissolved silica from waste water, comprising dispersing calcined hydrotalcite in an aqueous solution containing dissolved silica, whereby the hydrotalcite captures silicate ions from the aqueous solution.
2. The method of claim 1, wherein the hydrotalcite comprises [M.sup.(II).sub.1-xM.sup.(III).sub.x(OH).sub.2].sup.x+[A].mH.sub.2O where M.sup.(II)=Mg.sup.2+, Mn.sup.2+, Fe.sup.2+, Co.sup.2+, Ni.sup.2+, and Zn.sup.2+; M.sup.(III)=Al.sup.3+, Cr.sup.3+, Mn.sup.3+, Fe.sup.3+, Co.sup.3+, and Ga.sup.3+; and A=Cl.sup., Br.sup., I.sup., NO.sub.3.sup., CO.sub.3.sup.2, SO.sub.4.sup.2, silicate-, polyoxometalate-, and/or organic anions.
3. The method of claim 2, wherein the hydrotalcite comprises Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3).4H.sub.2O.
4. The method of claim 2, wherein the hydrotalcite comprises Zn.sub.6Al.sub.2(OH).sub.16.4H.sub.2O.
5. The method of claim 1, wherein the hydrotalcite is calcined at a temperature greater than 500 C.
6. The method of claim 1, wherein in the pH of the aqueous solution is greater than 9.5.
7. The method of claim 1, wherein the aqueous solution further comprises sulfate or chloride.
8. The method of claim 1, further comprising regenerating the hydrotalcite that is spent after capturing of the silicate ions from the aqueous solution.
9. The method of claim 8, wherein the regenerating comprising heating the spent hydrotalcite to a temperature greater than 500 C.
Description
BRIEF DESCRIPTION OF THE DRAWINGS
[0008] The detailed description will refer to the following drawings, wherein like elements are referred to by like numbers.
[0009]
[0010]
[0011]
[0012]
[0013]
[0014]
[0015]
[0016]
[0017]
[0018]
DETAILED DESCRIPTION OF THE INVENTION
[0019] Silica solubility depends on many factors, such as pH, temperature, pressure, and ionic strength. The silica solubility is constant between pH 2 and 8.5, but increases rapidly above pH 9. In the acidic-to-neutral pH range, silica exists as H.sub.4SiO.sub.4, whereas in basic solutions, it exists as H.sub.3SiO.sub.4.sup. and H.sub.2SiO.sub.4.sup.2 anionic species. See H.-H. Cheng et al., Separation and Purification Technology 70, 112 (2009); and I. Latour et al., Environmental Science and Pollution Research 23, 3707 (2015). Silica solubility is also highly sensitive to temperature, increasing from 100-140 mg/L at ambient temperature, and then up to 300 mg/L at 70 C. See I. Latour et al., Chemical Engineering Journal 230, 522 (2013).
[0020] Dissolved silica can be removed by a number of different methods including coagulation, nano-filtration (NF), reverse osmosis (RO), or precipitation. See I. Latour et al., Environmental Science and Pollution Research 23, 3707 (2015); I. Latour et al., Chemical Engineering Journal 230, 522 (2013); D. Hermosilla et al., Chemical Engineering & Technology 35, 1632 (2012); Y. Liu et al., Ind. Eng. Chem. Res. 51, 1853 (2012); and D. L. Gallup et al., Applied Geochemistry 18, 1597 (2003). Major limitations of NF and RO are fouling and high energy consumption. See S. Salvador Cob et al., Separation and Purification Technology 140, 23 (2015). The drawback of coagulation is that the process occurs at high pH, resulting in increased costs due to pH adjustment. See D. Hermosilla et al., Chemical Engineering & Technology 35, 1632 (2012). The current technology of alumina precipitation may cause aluminosilicate scaling. See S. Salvador Cob et al., Separation and Purification Technology 140, 23 (2015).
[0021] In an effort to develop highly selective silica ion-exchange materials that are robust, low cost and energy efficient, inorganic anion exchangers such as hydrotalcites (HTC) have been explored as silica adsorbents. HTCs are layered double-hydroxides with the general formula [M.sup.(II).sub.1-xM(III).sub.x(OH).sub.2].sup.x+[A].mH.sub.2O where M.sup.(II)=Mg.sup.2+, Mn.sup.2+, Fe.sup.2+, Co.sup.2+, Ni.sup.2+, and Zn.sup.2+; M.sup.(III)=Al.sup.3+, Cr.sup.3+, Mn.sup.3+, Fe.sup.3+, Co.sup.3+, and Ga.sup.3+; and A=Cl.sup., Br.sup., I.sup., NO.sub.3.sup., CO.sub.3.sup.2, SO.sub.4.sup.2, silicate-, polyoxometalate-, and/or organic anions. See A. Fahami and G. W. Beall, Journal of Solid State Chemistry 233, 422 (2016); and R. P. Bontchev et al., Chem. Mater 15, 3669 (2003). HTC is made up of positively charged [M.sup.(II)/M.sup.(III)/OH] layers, which have a substantial anion exchange capacity of 3 meq/g. See J. D. Pless et al., Ind. Eng. Chem. Res. 45, 4752 (2006); and D. Wan et al., Chemical Engineering Journal 195-196, 241 (2012). HTC has been shown to be a highly selective anion exchange material in a low energy, brackish water, desalination process. See J. D. Pless et al., Ind. Eng. Chem. Res. 45, 4752 (2006).
[0022] As shown in
HTC Characterization
[0023] As an example of the invention, 15 g batches of a commercially available HTC (Sigma-Aldrich), (Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3).4H.sub.2O), were calcined in air at 550 C. for 3 h. See D. G. Cantrell et al., Applied Catalysis A: General 287, 183 (2005). The surface area of the calcined HTC was 138 m.sup.2/g, whereas the surface area of the uncalcined HTC was 12 m.sup.2/g, as determined by the Brunauer-Emmet-Teller (BET) method. The higher surface area for calcined HTC can be a result of the decrease in HTC crystal size caused by thermal treatment, as shown in related studies. See K.-H. Goh et al., Water Research 42, 1343 (2008); and G. Fetter et al., Journal of Porous Materials 8, 227 (2001). This decrease in crystal size is supported by the broadening of powder X-ray diffraction (XRD) peaks for calcined HTC, as shown in
Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3).4H.sub.2O5MgO.MgAl.sub.2O.sub.4+CO.sub.2+H.sub.2O (1)
See J. C. Roelofs et al., ChemistryA European Journal 8, 5571 (2002). The calcined HTC can be reconstructed to its original structure when mixed in water containing anions of the correct size, charge and/or size in the interlayer of the recrystallized HTC. See H. Wang et al., Applied Clay Science 35, 59 (2007); and K. L. Erickson et al., Materials Letters 59, 226 (2005).
[0024] Thermogravimetric analysis (TGA) of uncalcined HTC shows that thermal decomposition of HTC takes place at two distinct steps. In Step I, the initial mass loss begins at room temperature and ends at 250 C., with 14% mass lost. This corresponds to the loss of water molecules located between the Mg/Al/OH layers. See L. Lv et al., Journal of Hazardous Materials 152, 1130 (2008). In Step II, the additional mass loss of 31% occurs between 250 C. and 510 C. Concurrent thermogravimetric-mass analysis (TGA-MS) indicates a mass loss of 7% is associated with carbonate anions, followed by gradual mass loss of 24% corresponding to loss of interlayer water molecules (condensation of OH groups from the Mg/Al/OH layers). See L. Lv et al., Journal of Hazardous Materials 152, 1130 (2008). The corresponding XRD shows the HTC becomes an amorphous phase upon calcination. The transition in the structural formulas during the two steps are: [0025] Step I: (Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3).4H.sub.2O)-4H.sub.2O(Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3)) (Calc. Wt. Loss=11.9%) [0026] Step II: (Mg.sub.6Al.sub.2(OH).sub.16(CO.sub.3))CO.sub.2-8H.sub.2O
5MgO.MgAl.sub.2O.sub.4 (Calc. Wt. Loss=31.2%)
[0027] As shown in
Mechanism of Silica Removal
[0028] Two different adsorption mechanisms have been used to describe the silica removal by HTC. The first process is direct ion-exchange with the interlayer anions of uncalcined HTC. See K.-H. Goh et al., Water Research 42, 1343 (2008). The second process, shown in
[0029] To understand which ion-exchange mechanism favors silica removal, both uncalcined HTC and calcined HTC were individually treated with synthetic industrial water (Concentrated Cooling Tower Water, CCTW). The CCTW was made by salt addition to DI water with the following concentrations (mmol/L): 0.41 MgCl.sub.2+0.05 Na.sub.2SO.sub.4+0.62 NaHCO.sub.3+1.0 CaCl.sub.2+41.0 NaCl+0.833 SiO.sub.2. For the batch silica removal reactions, typically 25-125 mg of HTC was added to 50 ml of the synthetic CCTW in 50 ml tubes, and the tube placed on a shaker table for 12 hours at room temperature. After shaking, the slurry was centrifuged, and the pH and silica concentration of the supernatant were determined. The percentage of silica removal was calculated based on the mass of silica removed by HTC to the initial mass of silica in water. The silica adsorption capacity is defined as the mass of silica removed from solution to the mass of calcined HTC used for silica removal.
[0030] As shown in
[0031] Silica adsorption by HTC as a function of time was also determined. In these experiments, 75 mg of calcined HTC was added to 50 ml of synthetic CCTW in a 50 ml tube; the tube was placed on shaker for a given time, up to 250 min. The resultant slurry was centrifuged, and silica concentration of the supernatant was determined by optical spectrophotometry.
Single Path Flow Through (SPFT) Measurement
[0032] A SPFT test was used to measure HTC uptake of silica under more rapid flow-through conditions and to provide a measure of uptake capacity. The SPFT measurement was done using synthetic CCTW and calcined HTC. See J. D. Pless et al., Ind. Eng. Chem. Res. 45, 4752 (2006). CCTW was pumped through columns containing 100-200 mg of calcined HTC at a flow rate of 0.15 ml min.sup.1. Treated CCTW effluent was periodically collected and the silica concentration and pH determined. The steady state volume of fluid in the reactor was 1 ml, which indicates an average fluid residence time of 7 minutes. As shown in
Effect of pH on Silica Removal by Calcined HTC
[0033] To measure the effect of pH, 25-125 mg of calcined HTC was added to 50 ml of the synthetic CCTW at pH 4-9 (the initial pH was adjusted by addition of 0.1 mol/L HCl or NaOH). The solution was placed on a shaker table for 12 hours at room temperature, then the slurry was centrifuged and the pH of solution was measured.
[0034] Changing the initial pH from 4 to 9 results in no significant effect on the silica removal performance by calcined HTC. Silica exists in the neutral form (H.sub.4SiO.sub.4) in the initial pH range (4-9), and is not available for ion-exchange. See N. A. Milne et al., Water Research 65, 107 (2014). As shown in
[0035] Changing the solution pH and the adsorption of silica ions by calcined HTC occurs as follows:
[0036] (1) OH ions are generated during reconstruction of HTC from magnesium and aluminum mixed oxides to the original crystalline structure. Concurrently, all available ions (Cl.sup., HCO.sub.3.sup., etc.) are adsorbed into the HTC interlayer, according to Eq. (2):
5MgO.MgAl.sub.2O.sub.4+13H.sub.2O+2Cl.sup.Mg.sub.6Al.sub.2(OH).sub.16Cl.sub.2.4H.sub.2O+2OH.sup.(2)
[0037] (2) As the pH rises to greater than 9.5, most of the silica is in the form of H.sub.3SiO.sub.4.sup. ions, as shown in
5MgO.MgAl.sub.2O.sub.4+13H.sub.2O+H.sub.3SiO.sub.4.sup.Mg.sub.6Al.sub.2(OH).sub.16(H.sub.3SiO.sub.4).sub.x.4HO.sub.2+2OH.sup.(3)
As shown in
Effect of Competing Ions on Silica Removal by Calcined HTC
[0038] Cooling tower water contains ions such as sulfate and chloride which might compete with silica for HTC adsorption sites. See W. Ma et al., Desalination 268, 20 (2011). Therefore, the ability of HTC to adsorb silica in the presence of competing anions was examined. To determine the effect of competing anions, binary solute systems of SiO.sub.2/SO.sub.4.sup.2 and SiO.sub.2/Cl.sup. (NaCl and Na.sub.2SO.sub.4 as sulfate and chloride sources), respectively, were measured with calcined HTC. Specifically, the binary-solute systems were mixed with the initial SiO.sub.2 concentration (50 mg/L) and the calcined HTC (125 mg). Table 1 shows that at silicate/chloride=1/20, 98% of dissolved silica was removed suggesting a strong preference of HTC for silicate over chloride. Similarly, at silicate/sulfate=1/20, 95% of the silicate was removed. The slightly lower silica removal in the presence of sulfate may be a due to the higher charge of SO.sub.4.sup.2 over Cl.sup.. See J. D. Pless et al., Ind. Eng. Chem. Res. 45, 4752 (2006). Overall, these results indicate that silica adsorption by calcined HTC is selective in the presence of competing ions, such as Cl.sup. and SO.sub.4.sup.2.
TABLE-US-00001 TABLE 1 Percent silica removal by HTC in presence of varying concentration of chloride and sulfate ions (initial silica concentration 50 mg/L, 50 ml, 125 mg HTC). Sample ratio Sample ratio Removed Silica:Chloride Removed silica (%) Silica:Sulfate Silica (%) 1:1 99.0% 1:1 99.0% 1:5 98.8% 1:5 97.0% 1:10 98.5% 1:10 95.8% 1:15 97.9% 1:15 95.2% 1:20 97.6% 1:20 94.8%
Regeneration of HTC
[0039] To determine the effect of HTC regeneration, the spent HTC was dried overnight in air at 60 C., and heated at 550 C. for 2 h. This process allowed for the regeneration of the crystalline HTC after each subsequent calcination for the silica removal process. The HTC after each subsequent calcination was used again for the removal of silicate anion from CCTW.
[0040] Regeneration cycling of the HTC involves cycles of calcination and reconstruction. Utilizing a non-optimized stoichiometry of the MgAl-HTC, no appreciable decrease in silica ion adsorption capacity was seen in the material after three recycles; a slight decrease was seen after the fourth cycle. Additional recycles allow for continued silica ion removal from the aqueous solution. The change in the sorption capacity was influenced by the ability of calcined HTC to regenerate the layered crystal structure during the ion-exchange process. As shown in
Kinetics of Silica Removal by Calcined HTC
[0041] The silica adsorption kinetics were best represented by a pseudo-second order equation, [t/q.sub.t=1/k.sub.2.sup.1qe.sup.2+t/q.sub.e], where k.sub.2.sup.1 (g/mg/min) is the pseudo-second order rate constant. See D. Folasegun Anthony et al., International journal of multidisciplinary sciences and engineering 3, 21 (2012); A. El Nemr et al., Arabian Journal of Chemistry 8, 105 (2015); and S. Nethaji et al., Bioresource Technology 134, 94 (2013). The values of t/q.sub.t plotted against given time (t) are shown in
[0042] Fitting this model implies that the rate of silica adsorption on the calcined HTC ion-exchanged sites is proportional to the square of the number of unoccupied active sites. See D. Folasegun Anthony et al., International journal of multidisciplinary sciences and engineering 3, 21 (2012). Since the ion-exchange kinetics is largely controlled by the active sites of calcined HTC available for sorption, the initial fast rate of ion-exchange, shown in
[0043] The present invention has been described as a method of removing dissolved silica from waste water. It will be understood that the above description is merely illustrative of the applications of the principles of the present invention, the scope of which is to be determined by the claims viewed in light of the specification. Other variants and modifications of the invention will be apparent to those of skill in the art.